| 屏边—西畴山弧地体南缘发现铜镍多金属硫化矿 |
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| 引用本文： | 张勤,杨玉华.屏边—西畴山弧地体南缘发现铜镍多金属硫化矿[J].云南地质,2012(2):139-143. |
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| 作者姓名： | 张勤 杨玉华 |
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| 作者单位： | 云南省有色地质局308队 |
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| 摘 要： | 眤博铜镍多金属矿处于哀牢山地体、红河裂陷槽、屏边西畴山弧交汇派生的北西多条线性断裂收敛区,辉长橄榄岩为铜镍钴容矿岩体。重磁推测基性岩体规模巨大,有较大远景。矿床类型为岩浆深部熔离—单成贯入式铜镍多金属矿。
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| 关 键 词： | 铜镍钴多金属矿 瑶山群一段赋矿 隐伏基性岩上部 垂直分带 云南河口瑶山 |
THE DISCOVERY OF CU-NI SULFIDE MULTIMETALLIC DEPOSIT AT S MARGIN OF PINGBIAN-XICHOU MOUNTAINOUS ARC TERRAIN |
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| ZHANG Qin,YANG Yu-hua.THE DISCOVERY OF CU-NI SULFIDE MULTIMETALLIC DEPOSIT AT S MARGIN OF PINGBIAN-XICHOU MOUNTAINOUS ARC TERRAIN[J].Yunnan Geology,2012(2):139-143. |
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| Authors: | ZHANG Qin YANG Yu-hua |
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| Institution: | (Geological Team 308,Yunnan Bureau of Nonferrous Geology,Gejiu 661400) |
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| Abstract: | The Nibo Cu-Ni multimetallic deposit is in the convergent area of many NW linear faults derived from the intersection of Ailaoshan terrain,Honghe fault depression trough and Pingbian-Xichou mountainous arc.The gabbroic peridotite is the rock body with Cu-Ni-Co rich ore body.According to the gravity and magnetic inference,the basic rock body is in large scale and considerable potentiality.It belongs to the type of immiscible of deep magma-simple injection Cu-Ni multimetallic deposit. |
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| Keywords: | Cu-Ni-Co Multimetallic Ore-bearing Yaoshan Group Member1 Upper Part of Buried Basic Rock Vertical Zonation Yaoshan Hekou Yunnan |
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